有机质供给和保存在烃源岩形成中的控制作用

丁修建; 柳广弟; 黄志龙; 卢学军; 陈哲龙; 谷峰

doi:10.3799/dqkx.2016.070

有机质供给和保存在烃源岩形成中的控制作用

doi: 10.3799/dqkx.2016.070

1.
中国石油大学地球科学与技术学院, 山东青岛 266580
2.
中国石油大学地球科学学院, 北京 102249
3.
中国石油华北油田分公司, 河北任丘 062550
4.
中海石油气电集团有限责任公司技术研发中心, 北京 100027

基金项目:

国家重点基础研究发展计划(973计划)项目 No.2014CB239005

国家科技重大专项项目 No.2011ZX05001-001

详细信息

作者简介:
丁修建(1986-), 男, 博士后, 主要从事油气藏形成与分布规律研究.E-mail：dingxj129@foxmail.com

中图分类号: P618.13
计量
- 文章访问数: 5569
- HTML全文浏览量: 2111
- PDF下载量: 45
- 被引次数: 0
出版历程
- 收稿日期: 2015-08-25
- 刊出日期: 2016-05-15

Ding Xiujian, Liu Guangdi, Huang Zhilong, Lu Xuejun, Chen Zhelong, Gu Feng

1.
School of Geosciences, China University of Petroleum, Qingdao 266580, China
2.
College of Geosciences, China University of Petroleum, Beijing 102249, China
3.
PetroChina Huabei Oilfield Company, Renqiu 062550, China
4.
Research and Development Center of Gas and Power Group, CNOOC Ltd., Beijing 100027, China

摘要

摘要: 烃源岩形成研究一直集中于海相盆地的“生产力模式”和“保存模式”之争, 湖相盆地研究较少.利用二连盆地烃源岩有机碳、碳酸盐碳同位素、热解参数、还原硫等地球化学分析数据, 表征了湖盆古生产力和陆源有机质输入, 研究了有机质供给和保存在烃源岩形成中的控制作用, 发现不同的湖盆中有机质供给和保存对烃源岩形成的控制作用明显不同.有机质供给量大的湖盆原始有机质含量高, 烃源岩形成主要受有机质供给控制, 受有机质保存条件影响小, 即使在含氧的水底也会有部分有机质来不及氧化而富集形成烃源岩; 有机质供给量小的湖盆原始有机质含量低, 氧化环境中大部分有机质被降解难以形成烃源岩, 只有还原环境下有机质才能得到较好的保存, 有机质保存是控制烃源岩形成的主要因素.
- 有机质供给 /
- 有机质保存 /
- 古生产力 /
- 陆源有机质输入 /
- 二连盆地 /
- 石油地质.
Abstract: The debate on formation of source rocks has been focused on "productivity mode" and "preservation mode" in marine sediments for many years. Based on the datasets of total organic carbon, carbonate carbon isotope, pyrolysis parameters and reduced sulfur of source rocks of Erlian basin, the productivity and terrigenous organic matter input are characterized and then the role of organic matter supply and preservation in the formation of source rocks are discussed. For the lacustrine basin with high organic matter supply, organic matter supply is the main factor controlling the formation on source rocks because there are still source rocks formed by accumulation of residual organic matter even in the oxidizing sedimentary environment. For the lacustrine basin with low organic matter supply, preservation is the main factor controlling the formation on source rocks because the organic matter can only be preserved in reducing environment since it is too rare to be preserved from oxidation.
- organic matter supply /
- organic matter preservation /
- paleo-productivity /
- terrigenous organic matter input /
- Erlian basin /
- petroleum geology.

HTML全文

图 1 二连盆地构造单元划分及研究区位置

Fig. 1. Tectonic units of Erlian basin and the location of study area

下载: 全尺寸图片幻灯片

图 2 二连盆地典型地质剖面

剖面位置见图 1

Fig. 2. Representative section showing the structural framework of Erlian basin

下载: 全尺寸图片幻灯片

图 3 二连盆地地层综合柱状图

据华北油田内部资料(2009)修改

Fig. 3. Generalized stratigraphic column of Erlian basin

下载: 全尺寸图片幻灯片

图 4 烃源岩原地有机质比例判识

Fig. 4. Identification for in-situ oganic matter ratio of source rock

下载: 全尺寸图片幻灯片

图 5 二连盆地总有机质供给指数与有机碳含量关系

Fig. 5. Relationship between total organic matter supply index and total organic carbon content in Erlian basin

下载: 全尺寸图片幻灯片

图 6 二连盆地烃源岩U/Th分布频率直方图

Fig. 6. U/Th values in source rocks, Erlian basin

下载: 全尺寸图片幻灯片

图 7 二连盆地还原S与烃源岩有机碳含量关系

Fig. 7. Relationships between reducing S content and total organic carbon content in Erlian basin

下载: 全尺寸图片幻灯片

表 1 二连盆地有机质供给指数

Table 1. Organic matter supply index in Erlian basin

凹陷	井号	深度(m)	δ¹³C(PDB，‰)	原地有机质生产指数	原地有机质比例	陆源有机质输入指数	总有机质供给指数	TOC(%)
阿尔	阿尓1	1 467.4	4.551	0.69	0.65	0.37	1.07	1.27
	阿尓1	1 798.0	-1.667	0.38	0.35	0.70	1.08	0.83
	阿尓5	1 912.4	4.885	0.71	0.70	0.30	1.02	0.79
	阿尓6	1 652.1	7.714	0.86	0.35	1.59	2.45	1.80
	阿尔3	1 640.8	5.130	0.72	0.15	4.10	4.83	1.48
	阿尓2	1 910.6	-2.566	0.33	0.20	1.33	1.66	0.44
	阿尓21	1 495.5	-5.343	0.19	0.10	1.71	1.90	0.90
	阿尓5	1 928.4	4.591	0.70	0.15	3.95	4.64	2.43
乌里雅斯太	太11	1 587.3	6.934	0.82	0.15	4.62	5.44	3.30
	太3	1 399.1	2.697	0.60	0.30	1.40	2.00	1.95
	太65	2 455.5	-0.699	0.43	0.10	3.84	4.27	2.24
	太75	1 269.5	-6.193	0.15	0.10	1.32	1.46	0.53
	太87	553.3	-6.087	0.15	0.15	0.86	1.01	0.09
额仁淖尔	淖120	1 674.0	0.015	0.46	0.25	1.39	1.85	1.02
	淖16	1 799.7	3.235	0.63	0.26	1.79	2.41	0.42
	淖3	736.7	-1.459	0.39	0.25	1.16	1.55	0.43
	淖6	1 428.3	2.022	0.57	0.45	0.69	1.26	0.89
	淖6	1 426.7	2.616	0.60	0.35	1.11	1.70	1.47
	淖68	1 733.3	-0.148	0.45	0.25	1.36	1.82	0.65
	淖81	887.2	-4.455	0.23	0.15	1.33	1.57	0.15
赛汉塔拉	赛27	1 660.5	6.690	0.80	0.50	0.80	1.61	1.97
	赛80	2 200.0	1.171	0.52	0.25	1.57	2.09	1.19
	赛20	917.2	-2.674	0.33	0.25	0.98	1.30	1.11
	赛27	2 220.3	-4.124	0.25	0.15	1.43	1.68	0.08
	赛4	1 011.9	-3.336	0.29	0.12	2.14	2.43	0.49
	赛4	949.7	-2.711	0.32	0.60	0.22	0.54	0.10
	赛4	829.1	0.722	0.50	0.25	1.50	2.00	0.33
	赛52	1 444.3	-3.584	0.28	0.15	1.58	1.86	0.11
	赛56	1 479.5	0.048	0.46	0.25	1.39	1.86	1.14
	赛63	1 329.5	0.829	0.50	0.32	1.07	1.58	2.02
	赛69	1 428.6	0.790	0.50	0.25	1.51	2.01	0.44

下载: 导出CSV

参考文献(74)

Adegoke A.K., Abdullah W.H., Hakimi M.H., et al.2014.Geochemical Characterisation of Fika Formation in the Chad (Bornu) Basin, Northeastern Nigeria:Implications for Depositional Environment and Tectonic Setting[J].Applied Geochemistry, 43:1-12.doi: 10.1016/j.apgeochem.2014.01.008
Arthur M.A., Dean W.E..1998.Organic-Matter Production and Preservation and Evolution of Anoxia in the Holocene Black Sea[J].Paleoceanography, 13(4):395-411.doi:10.1029/98pa01161
Calvert S.E..1987.Oceanographic Controls on the Accumulation of Organic Matter in Marine Sediments[J].Geological Society, London, Special Publications, 26(1):137-151.doi:10.1144/gsl.sp.1987.026.01.08
Calvert S.E., Bustin R.M., Pedersen T.F..1992.Lack of Evidence for Enhanced Preservation of Sedimentary Organic Matter in the Oxygen Minimum of the Gulf of California[J].Geology, 20(8):757.doi:10.1130/0091-7613(1992)020<0757:loefe >2.3.co;2
Calvert S.E., Pedersen T.F., Naidu P.D., et al.1995.On the Organic Carbon Maximum on the Continental Slope of the Eastern Arabian Sea[J].Journal of Marine Research, 53(2):269-296.doi: 10.1357/0022240953213232
Calvert S.E., Pedersen T.F..1990.Anoxia vs.Productivity:What Controls the Formation of Organic-Carbon-Rich Sediments and Sedimentary Rocks? (1)[J].AAPG Bulletin, 74:454-466.doi: 10.1306/0c9b232b-1710-11d7-8645000102c1865d
de Graciansky P.C., Deroo G., Herbin J.P., et al.1984.Ocean-Wide Stagnation Episode in the Late Cretaceous[J].Nature, 308(5957):346-349.doi: 10.1038/308346a0
Degens E.T., von Herzen R.P.V., Wong H.K..1971.Lake Tanganyika:Water Chemistry, Sediments, Geological Structure[J].Naturwissenschaften, 58(5):229-241.doi:10.1007/bf00602986
Degens E.T., von Herzen R.P.V., Wong H.K., et al.1973.Lake Kivu:Structure, Chemistry and Biology of an East African Rift Lake[J].Geologische Rundschau, 62(1):245-277.doi:10.1007/bf01826830
Demaison G.J., Moore G.T..1980.Anoxic Environments and Oil Source Bed Genesis[J].Organic Geochemistry, 2(1):9-31.doi: 10.1016/0146-6380(80)90017-0
Fang J., Hou F.X., Sun T.T., et al.1998a.Thermal Evolution Characteristic of Organic Matter of Lower Cretaceous Source Rock in Erlian Rift System[J].Xinjiang Petroleum Geology, 19(6):476-479 (in Chinese with English abstract). doi: 10.1007/s12182-014-0348-z
Fang J., Yu Z.W., Shen J.M., .1998b.Organic Matter Types and Organic Facies of Hydrocarbon Source Rock in Erlian Basin[J].Journal of Xi'an Petroleum Institute, 13(5):11-16 (in Chinese with English abstract). https://www.researchgate.net/publication/285740517_Organic_matter_types_and_organic_facies_of_hydrocarbon_source_rock_in_Erlian_Basin
Gucluer S.M., Gross M.G..1964.Recent Marine Sediments in Saanich Inlet, a Stagnant Marine Basin[J].Limnology and Oceanography, 9(3):359-376.doi: 10.4319/lo.1964.9.3.0359
Hao F., Zhou X.H., Zhu Y.M., et al.2011.Lacustrine Source Rock Deposition in Response to Co-Evolution of Environments and Organisms Controlled by Tectonic Subsidence and Climate, Bohai Bay Basin, China[J].Organic Geochemistry, 42(4):323-339.doi: 10.1016/j.orggeochem.2011.01.010
Hedges J.I., Keil R.G..1995.Sedimentary Organic Matter Preservation:An Assessment and Speculative Synthesis[J].Marine Chemistry, 49(2-3):81-115.doi:10.1016/0304-4203(95)00008-f
Hollis C.J., Tayler M.J.S., Andrew B., et al.2014.Organic-Rich Sedimentation in the South Pacific Ocean Associated with Late Paleocene Climatic Cooling[J].Earth-Science Reviews, 134:81-97.doi: 10.1016/j.earscirev.2014.03.006
Huang D.F..1979.A Comprehensive Survey Report on the Qinghai Lake.Science Press, Beijing 152-156(in Chinese).
Jin Q., Zhu G.Y., Wang J..2008.Deposition and Distribution of High-Potential Source Rocks in Saline Lacustrine Enviroments[J].Journal of China University of Petroleum, 32(4):19-23 (in Chinese with English abstract). https://www.researchgate.net/publication/249548730_Environments_of_deposition_of_lacustrine_petroleum_source_rocks_an_introduction_In_Fleet_A_J_Kelts_K_and_Talbot_M_R_Eds_Lacustrine_Petroleum_Source_Rocks
Katz B.J..1990.Controls on Distribution of Lacustrine Source Rocks through Time and Space.In:Katz B.J., ed., Lacustrine Basin Exploration:Case Studies and Modern Analogs, AAPG Memoir 50.AAPG, Tusal, 61-76. http://www.sciencedirect.com/science/article/pii/S0037073816303025
Katz B.J..2005.Controlling Factors on Source Rock Development—A Review of Productivity, Preservation, and Sedimentation Rate[J].Deposition of Organic-Carbon-Rich Sediments:Models, 74:7-16.doi: 10.2110/pec.05.82.0007
Kimura H., Watanabe Y..2001.Oceanic Anoxia at the Precambrian-Cambrian Boundary[J].Geology, 29(11):995.doi:10.1130/0091-7613(2001)029<0995:oaatpc>2.0.co;2
Li S.F., Xu S.H., Shi H.S., et al.2013.Characteristics of Paleogene Source Rocks and Prediction of Petroleum Resources in Huizhou Depression, Pearl River Mouth Basin[J].Earth Science, 38(1):112-120(in Chinese with English abstract). https://www.researchgate.net/publication/291103351_Characteristics_and_genesis_of_mudstone_compaction_in_Huizhou_Depression_Pearl_River_Mouth_Basin
Liang D.G..2001.Petroleum Generation of Jizhong Depression.Petroleum Industry Press, Beijing 111-112(in Chinese).
Ma L.Q., 2005 Sequence Stratigraphy Research and Stratigraphic/Lithologic Reservoirs Prediction on Lower Cretaceous in A'nan-Abei Sag, Erlian Basin, China (Dissertation).Zhejiang University, Hangzhou (in Chinese with English abstract).
Mazzini A., Ivanov M.K., Nermoen A., et al.2008.Complex Plumbing Systems in the near Subsurface:Geometries of Authigenic Carbonates from Dolgovskoy Mound (Black Sea) Constrained by Analogue Experiments[J].Marine and Petroleum Geology, 25(6):457-472.doi: 10.1016/j.marpetgeo.2007.10.002
McKenzie J.A..1982.Carbon-13 Cycle in Lake Greifen:A Model for Restricted Ocean Basins.In:Schlanger S.O., Cita M.B., eds., Nature and Origin of Cretaceous Carbon Rich Facies.Academic Press, London, 197-207.
McKenzie J.A..1985.Carbon Isotopes and Productivity in the Lacustrine and Marine Environment.In:Stumm W., ed., Chemical Processes in Lakes.Wiley, New York, 99-118. doi: 10.1007/0-306-48201-0_18
McManus J., Berelson W.M., Klinkhammer G.P., et al.2005.Authigenic Uranium:Relationship to Oxygen Penetration Depth and Organic Carbon Rain[J].Geochimica et Cosmochimica Acta, 69(1):95-108.doi: 10.1016/j.gca.2004.06.023
Morford J.L., Russell A.D., Emerson S..2001.Trace Metal Evidence for Changes in the Redox Environment Associated with the Transition from Terrigenous Clay to Diatomaceous Sediment, Saanich Inlet, BC[J].Marine Geology, 174(1-4):355-369.doi:10.1016/s0025-3227(00)00160-2
Oana S., Deevey E.S..1960.Carbon 13 in Lake Waters and Its Possible Bearing on Paleolimnology[J].American Journal of Science, 258:253-272. doi: 10.1023/A:1005702707183
Parrish J.T..1995.Paleogeography of Corg-Rich Rocks and the Preservation versus Production Controversy.In:Huc A.Y., ed., Paleogeography, Paleoclimate, and Source Rock:American Association of Petroleum Geologists[J].Studies in Geology, 40:1-20. doi: 10.2307/3515771
Ren Z.L., Feng J.H., Liu C.Y., et al.2000.Organic Geochemical Feature of Lower Cretaceous Source Rock in Bayindulan Depression of Erlian Basin[J].Journal of Northwest University (Nature Science Edition), 30(4):328-331 (in Chinese with English abstract). doi: 10.1007/s12303-016-0061-6
Richards F.A., Vaccaro R.F..1956.The Cariaco Trench, an Anaerobic Basin in the Caribbean Sea[J].Deep Sea Research(1953), 3(3):214-228.doi: 10.1016/0146-6313(56)90005-3
Stein R..1986.Organic Carbon and Sedimentation Rate—Further Evidence for Anoxic Deep-Water Conditions in the Cenomanian/Turonian Atlantic Ocean[J].Marine Geology, 72(3-4):199-209.doi: 10.1016/0025-3227(86)90119-2
Stein R..1990.Organic Carbon Content/Sedimentation Rate Relationship and Its Paleoenvironmental Significance for Marine Sediments[J].Geo-Marine Letters, 10(1):37-44.doi:10.1007/bf02431020
Tian F.Q..2008.Source Rocks and Oil-Source Rock Correlation in the Bayindulan Sag of Erlian Basin[J].Natural Gas Geoscience, 19(4):541-543, 565(in Chinese with English abstract). doi: 10.1007/s12303-016-0061-6
Tyson R.V..1987.The Genesis and Palynofacies Characteristics of Marine Petroleum Source Rocks[J].Geological Society, London, Special Publications, 26(1):47-67.doi:10.1144/gsl.sp.1987.026.01.03
Tyson R.V., Pearson T.H..1991.Modern and Ancient Continental Shelf Anoxia:An Overview.In:Tyson R.V., Pearson T.H., eds., Modern and Ancient Continental Shelf Anoxia[J].Geological Society, London, Special Publication, 58:1-24. doi: 10.1144/GSL.SP.1991.058.01.01
van Bentum E.C.V., Reichart G.J., Damsté J.S.S..2012.Organic Matter Provenance, Palaeoproductivity and Bottom Water Anoxia during the Cenomanian/Turonian Oceanic Anoxic Event in the Newfoundland Basin (Northern Proto North Atlantic Ocean)[J].Organic Geochemistry, 50:11-18.doi: 10.1016/j.orggeochem.2012.05.013
Wang P.X..1989.Introduction to Paleoceanography.Tongji University Press, Shanghai, 17(in Chinese). https://www.researchgate.net/publication/298799046_Introduction_to_Pliocene-Pleistocene_Paleoceanography_of_the_Bering_Sea
Wang Q..2010.The Main Distribution Zone and Reservoir Forming Mechanism of Lithologic Reservoirs in Oil-Bearing Fault Sags, Erlian Basin(Dissertation).China University of geosciences, Beijing (in Chinese with English abstract). https://www.researchgate.net/publication/308185401_Fine-grained_and_coarse-grained_Paleogene_sublacustrine_fan_systems_in_Fushan_Depression_Beibuwan_Basin_South_China_Sea_implications_for_sedimentary_characteristics_and_depositional_processes
Wang T.H..1986.A Preliminary Study on the Erlian Basin Characteristics for Structural Petroleum Geological[J].Experimental Petroleum Geology, 8(4):313-324 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYSD198604003.htm
Wang X.D., Jiang Z.X., Pang X.Q..2003.Summarization of the Paleohydrocarbon-Water Contact Restoring Methods[J].Advance in Earth Sciences, 18(3):412-419(in Chinese with English abstract). doi: 10.11867/j.issn.1001-8166.2003.03.0412
Wignall P.B., Twitchett R.J..1996.Oceanic Anoxia and the End Permian Mass Extinction[J].Science, 272(5265):1155-1158.doi: 10.1126/science.272.5265.1155
Wu G.X., Zhu W.L., Li M.B., et al.1999.Important Factor Controlling the Development of Rich Oil Kitchen Sags:Anoxic Conditions—Evidences from the Pearl River Mouth Basin[J].China Offshore Oil and Gas(Geology), 13(1):1-6(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYXB199202013.htm
Xiao Y., Tang J., Sun C.H., et al.2010.Hydrocarbon Accumulation Conditions and Reservoir Types of Aer Sag in Erlian Basin[J].China Petroleum Exploration, 15(2):41-44(in Chinese with English abstract).doi: 10.3969/j.issn.1672-7703.2010.02.008
Yao Y.J., Lü C.L., Kang Y.S., et al.2013.Characteristics of Hydrocarbon Source Rocks and Their Main Controlling Factors in Southeast Asia[J].Earth Science, 38(2):365-378(in Chinese with English abstract). https://www.researchgate.net/publication/287434521_Characteristics_of_hydrocarbon_source_rocks_and_their_main_controlling_factors_in_Southeast_Asia
Yu Y.T..1990.Evolution Characteristics of Erlian Basin and the Distribution of Oil and Gas Deposits[J].Acta Petrolei Sinica, 11(3):12-20 (in Chinese with English abstract). https://www.researchgate.net/publication/290484613_Evolution_characteristics_of_Erlian_Basin_and_the_distribution_of_oil_and_gas_deposits
Zhang Z.L., Miao W.D., Chen K.Y..2008.Hydrocarbon Genesis in Honghao'ershute Depression of Erlian Basin[J].Journal of Oil and Gas Technology, 30(2):178-181 (in Chinese with English abstract). http://manu39.magtech.com.cn/Geophy/EN/abstract/abstract8950.shtml
Zhao X.Z., Jiang S.Q., Dan W.N., et al.2010a.Petroleum Geologic Characteristics of Artala Sag in Erlian Basin[J].Lithologic Reservoirs, 22(1):12-17(in Chinese with English abstract).doi: 10.3969/j.issn.1673-8926.2010.01.003
Zhao X.Z., Shi Y.P., Jiang S.Q., et al.2010b.Scientific, Fast, and Efficient Exploration in Aer Sag of Erlian Basin[J].China Petroleum Exploration, 15(1):1-5(in Chinese with English abstract).doi: 10.3969/j.issn.1672-7703.2010.01.001
Zhu Y.H., Zhang W.C..2000.Sedimentary Facies and Hydrocarbon-Bearing of Lower Cretaceous Strata in Erlian Basin.Science Press, Beijing, 81-162(in Chinese). https://www.researchgate.net/publication/281701196_Coupling_of_faulted_sags_to_basement_in_the_Early_Cretaceous_Erlian_Basin
Zonneveld K.A.F., Versteegh G.J.M., Kasten S., et al.2010.Selective Preservation of Organic Matter in Marine Environments:Processes and Impact on the Sedimentary Record[J].Biogeosciences, 7(2):483-511.doi: 10.5194/bg-7-483-2010
方杰, 侯凤香, 孙彤彤, 等.1998a.二连裂谷系下白垩统烃源岩有机质热演化特征.新疆石油地质, 19(6):476-479. http://www.cnki.com.cn/Article/CJFDTOTAL-XJSD806.008.htm
方杰, 鱼占文, 沈敬茂.1998b.二连盆地烃源岩有机质类型及有机相.西安石油学院学报:自然科学版, 13(5):11-16. http://www.cnki.com.cn/Article/CJFDTOTAL-XASY805.002.htm
黄第藩.1979.青海湖综合考察报告.北京:科学出版社, 152-156.
金强, 朱光有, 王娟.2008.咸化湖盆优质烃源岩的形成与分布.中国石油大学学报, 32(4):19-23. http://www.cnki.com.cn/Article/CJFDTOTAL-SYDX200804005.htm
李松峰, 徐思煌, 施和生, 等.2013.珠江口盆地惠州凹陷古近系烃源岩特征及资源预测.地球科学, 38(1):112-120. http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201301015.htm
梁狄刚.2001.冀中坳陷油气的生成.北京:石油工业出版社, 111-112.
马立桥. 2005. 二连盆地阿南-阿北凹陷下白垩统层序发育特征与岩性地层油气藏预测(博士学位论文). 杭州: 浙江大学. http://www.cnki.com.cn/Article/CJFDTOTAL-TZCZ199903009.htm
任战利, 冯建辉, 刘池洋, 等.2000.巴音都兰凹陷烃源岩有机地球化学特征.西北大学学报:自然科学版, 30(4):328-331. http://www.cnki.com.cn/Article/CJFDTOTAL-XBDZ200004017.htm
田福清.2008.二连盆地巴音都兰凹陷烃源岩评价及油源研究.天然气地球科学, 19(4):541-543, 565. doi: 10.11764/j.issn.1672-1926.2008.04.541
汪品先.1989.古海洋学概论.上海:同济大学出版社, 17.
王权.2010.二连盆地含油断陷岩性油藏主要发育区带与成藏机制研究(博士学位论文).北京:中国地质大学.
王同和.1986.二连盆地石油地质构造特征初探.石油实验地质, 8(4):313-324. doi: 10.11781/sysydz198604313
王显东, 姜振学, 庞雄奇.2003.古油气水界面恢复方法综述.地球科学进展, 18(3):412-419. http://www.cnki.com.cn/Article/CJFDTOTAL-DXJZ200303013.htm
吴国瑄, 朱伟林, 黎明碧, 等.1999.古湖缺氧条件是控制富生油凹陷形成的重要因素——来自珠江口盆地的证据.中国海上油气(地质), 13(1):1-6. http://www.cnki.com.cn/Article/CJFDTOTAL-ZHSD199901000.htm
肖阳, 唐谨, 孙朝辉, 等.2010.二连盆地阿尔凹陷油气成藏条件及油藏类型.中国石油勘探, 15(2):41-44. http://www.cnki.com.cn/Article/CJFDTOTAL-KTSY201002008.htm
姚永坚, 吕彩丽, 康永尚, 等.2013.东南亚地区烃源岩特征与主控因素.地球科学, 38(2):367-378. http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201302019.htm
于英太.1990.二连盆地演化特征及油气分布.石油学报, 11(3):12-20. doi: 10.7623/syxb199003002
张志琳, 缪卫东, 陈开远.2008.二连盆地洪浩尔舒特凹陷油气生成.石油天然气学报, 30(2):178-181. http://www.cnki.com.cn/Article/CJFDTOTAL-JHSX200802045.htm
赵贤正, 降栓奇, 淡伟宁, 等.2010a.二连盆地阿尔凹陷石油地质特征研究.岩性油气藏, 22(1):12-17. http://www.cnki.com.cn/Article/CJFDTOTAL-YANX201001006.htm
赵贤正, 史原鹏, 降栓奇, 等.2010b.二连盆地阿尔凹陷科学、快速、高效勘探实践和认识.中国石油勘探, 15(1):1-5. http://www.cnki.com.cn/Article/CJFDTOTAL-KTSY201001002.htm
祝玉衡, 张文朝.2000.二连盆地下白垩统沉积相及含油性.北京:科学出版社, 81-162.